No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha39","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1960, Floods near Chicago Heights, Illinois: U.S. Geological Survey Hydrologic Atlas 39, 1 Plate: 30.50 × 30.00 inches, https://doi.org/10.3133/ha39.","productDescription":"1 Plate: 30.50 × 30.00 inches","costCenters":[],"links":[{"id":185621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388450,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15770.htm"},{"id":89892,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinois","city":"Chicago Heights","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.61749999999999,41.5 ], [ -87.61749999999999,41.6175 ], [ -87.5,41.6175 ], [ -87.5,41.5 ], [ -87.61749999999999,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e07ed","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3551,"text":"cir425 - 1960 - Are you concerned about water?--you will be","interactions":[],"lastModifiedDate":"2018-01-02T20:38:33","indexId":"cir425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"425","title":"Are you concerned about water?--you will be","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir425","usgsCitation":"Piper, A., 1960, Are you concerned about water?--you will be: U.S. Geological Survey Circular 425, 6 p. ;27 cm., https://doi.org/10.3133/cir425.","productDescription":"6 p. ;27 cm.","costCenters":[],"links":[{"id":30571,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0425/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f46","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":147145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3499,"text":"cir423 - 1960 - Occurrence of ground waters of low hardness and of high chloride content in Lyon County, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:13:04","indexId":"cir423","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"423","title":"Occurrence of ground waters of low hardness and of high chloride content in Lyon County, Minnesota","docAbstract":"The ground water in Lyon County and elsewhere in southwestern Minnesota is generally hard and low in chloride. It is the purpose of this report to describe briefly the occurrence in Lyon County of waters of low hardness and of high chloride content. The waters are found largely in Cretaceous sandstone.
\nThe data were collected in conjunction with a countywide study of the geology and groundwater resources that is being made as part of a statewide investigation in cooperation with the Division of Waters, Minnesota Department of Conservation. The work is under the direct supervision of the junior author, who is district geologist for Minnesota.
\nHardness and chloride determinations were made with field-testing kits at the time data were obtained on most of the farm wells in the county. Tests were made on wells that were reported to yield relatively soft or \"salty\" water.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir423","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Rodis, H.G., and Schneider, R., 1960, Occurrence of ground waters of low hardness and of high chloride content in Lyon County, Minnesota: U.S. Geological Survey Circular 423, iii, 2 p., https://doi.org/10.3133/cir423.","productDescription":"iii, 2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":120863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0423/report-thumb.jpg"},{"id":30509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Lyon County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.0914,44.631],[-95.6023,44.6309],[-95.6028,44.5433],[-95.5938,44.5434],[-95.5921,44.1964],[-96.0628,44.1987],[-96.0788,44.1993],[-96.0747,44.5455],[-96.0932,44.5456],[-96.0914,44.631]]]},\"properties\":{\"name\":\"Lyon\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db6923bd","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147041,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":147042,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3435,"text":"cir420 - 1960 - Occurrence of strontium in natural water","interactions":[],"lastModifiedDate":"2017-02-21T16:15:35","indexId":"cir420","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"420","title":"Occurrence of strontium in natural water","docAbstract":"The regions where the stable strontium content of surface waters is relatively low (less than 0.50 ppm) include the Pacific Northwest, Northeastern United States, and the Central Lowlands, Particularly the Lower Mississippi basin and the Western Gulf Coast area. Moderate concentrations of strontium (0.50 to 1.5 ppm) are found in streams of Southeastern United States, most of the Great Plains Region, the Western Mountain and Plateau Regions, and California. Relatively high concentrations of strontium occur in the surface waters of an area that includes Northern and Western Texas and Southern New Mexico and Arizona. Exceptions to the above distribution are due to local geologic conditions.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir420","usgsCitation":"Skougstad, M., and Horr, C.A., 1960, Occurrence of strontium in natural water: U.S. Geological Survey Circular 420, iii, 6 p., https://doi.org/10.3133/cir420.","productDescription":"iii, 6 p.","numberOfPages":"11","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":30450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0420/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0420/report-thumb.jpg"}],"country":"United States","publicComments":"Prepared on behalf of the U. S. Atomic Energy Commission and published with the permission of the Commission","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69219d","contributors":{"authors":[{"text":"Skougstad, M. W.","contributorId":59418,"corporation":false,"usgs":true,"family":"Skougstad","given":"M. W.","affiliations":[],"preferred":false,"id":146907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horr, C. Albert","contributorId":43333,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39058,"text":"pp334G - 1960 - Dispersion characteristics of montmorillonite, kaolinite, and illite clays in waters of varying quality, and their control with phosphate dispersants","interactions":[],"lastModifiedDate":"2012-02-02T00:09:59","indexId":"pp334G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"334","chapter":"G","title":"Dispersion characteristics of montmorillonite, kaolinite, and illite clays in waters of varying quality, and their control with phosphate dispersants","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1958","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp334G","usgsCitation":"Rolfe, B., Miller, R., and McQueen, I., 1960, Dispersion characteristics of montmorillonite, kaolinite, and illite clays in waters of varying quality, and their control with phosphate dispersants: U.S. Geological Survey Professional Paper 334, p. 229-273, https://doi.org/10.3133/pp334G.","productDescription":"p. 229-273","costCenters":[],"links":[{"id":122140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0334g/report-thumb.jpg"},{"id":66288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0334g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a31c","contributors":{"authors":[{"text":"Rolfe, B.N.","contributorId":80333,"corporation":false,"usgs":true,"family":"Rolfe","given":"B.N.","email":"","affiliations":[],"preferred":false,"id":220875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":220876,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McQueen, I.S.","contributorId":59774,"corporation":false,"usgs":true,"family":"McQueen","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":220874,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1227,"text":"wsp1480 - 1960 - Evaporation control research, 1955-58","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1480","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1480","title":"Evaporation control research, 1955-58","docAbstract":"One hundred fifty-two compounds and compositions of matter were screened as potential evaporation retardants. The homologous straight-chain fatty alkanols are considered the best materials for retardants. \r\n\r\nSeveral methods of application of the alkanols to the reservoir surface were investigated. Although wick-type drippers for the application of liquids and cage rafts for the application of solids appear to be the most promising methods from an economic standpoint, both methods have serious disadvantages. Considerable study was given to reducing biochemical oxidation of the evaporation retardants. Copper in several forms was found adequate as a bacteriostatic agent but posed a potential hazard because of its toxicity. Many other bactericides that were tested were also toxic. \r\n\r\nTwo sets of large-scale field tests have been completed and several others are still in progress. On the larger reservoirs, the reduction of evaporation was not more than 20 percent under the prevailing conditions and the application procedure used. \r\n\r\nThree major practical problems remain; namely, the effects and action of wind on the monofilm, the effects of biochemical oxidation, and the most effective method of application. Fundamental problems remaining include the effects of various impurities, and the composition of the best evaporation retardant; the long-range effects of monofilms on the limnology of a reservoir, including the transfer of oxygen and carbon dioxide; toxicological aspects of all components of any evaporation-retardant composition, plus toxicology of any composition chosen for large-scale use; and further studies of the calorimetry and thermodynamics involved in the mechanism of evaporation and its reduction by a monofilm.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1480","usgsCitation":"Cruse, R.R., and Harbeck, G.E., 1960, Evaporation control research, 1955-58: U.S. Geological Survey Water Supply Paper 1480, iv, 45 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1480.","productDescription":"iv, 45 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1480/report-thumb.jpg"},{"id":26145,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9433","contributors":{"authors":[{"text":"Cruse, Robert R.","contributorId":93326,"corporation":false,"usgs":true,"family":"Cruse","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbeck, Guy Earl","contributorId":82290,"corporation":false,"usgs":true,"family":"Harbeck","given":"Guy","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":143402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1236,"text":"wsp1543A - 1960 - Flood-frequency analyses, Manual of Hydrology: Part 3","interactions":[{"subject":{"id":22463,"text":"ofr5813 - 1958 - Characteristics of frequency curves based on a theoretical 1,000-year record","indexId":"ofr5813","publicationYear":"1958","noYear":false,"title":"Characteristics of frequency curves based on a theoretical 1,000-year record"},"predicate":"SUPERSEDED_BY","object":{"id":1236,"text":"wsp1543A - 1960 - Flood-frequency analyses, Manual of Hydrology: Part 3","indexId":"wsp1543A","publicationYear":"1960","noYear":false,"chapter":"A","title":"Flood-frequency analyses, Manual of Hydrology: Part 3"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1543A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1543","chapter":"A","title":"Flood-frequency analyses, Manual of Hydrology: Part 3","docAbstract":"This report describes the method used by the U.S. Geological Survey to determine the magnitude and frequency of momentary peak discharges at any place on a stream, whether a gaging-station record is available or not. The method is applicable to a region of any size, as a river basin or a State, so long as the region is hydrologically homogeneous. \r\n\r\nThe analysis provides two curves. The first expresses the flood discharge-time relation, showing variation of peak discharge, expressed as a ratio to the mean annual flood, with recurrence interval. The second relates the mean annual flood to the size of drainage area alone, or to the size area and other significant basin characteristics. \r\n\r\nA frequency curve may be defined for any place in the region by use of these two curves. The procedure is: (a) measure the drainage area and other appropriate basin characteristics from maps; (b) from the second curve, select the mean annual flood corresponding to the proper drainage area factors; (c) from the first curve, select ratios of peak discharge to mean annual flood for selected recurrence intervals, as 2, 10, 25, and 50 years; and (d) multiply these ratios by the mean annual flood and plot the resulting discharges of known frequency to define the frequency curve. \r\n\r\nTwo reports not previously given general circulation are included as sections of this report. These are 'Plotting Positions in Frequency Analysis' by W. B. Langbein, and 'Characteristics of Frequency Curves Based on a Theoretical 1,000-Year Record' by M. A. Benson.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1543A","usgsCitation":"Dalrymple, T., 1960, Flood-frequency analyses, Manual of Hydrology: Part 3: U.S. Geological Survey Water Supply Paper 1543, v, 80 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1543A.","productDescription":"v, 80 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":138088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1543a/report-thumb.jpg"},{"id":26164,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1543a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4884e4b07f02db5189fd","contributors":{"authors":[{"text":"Dalrymple, Tate","contributorId":59420,"corporation":false,"usgs":true,"family":"Dalrymple","given":"Tate","email":"","affiliations":[],"preferred":false,"id":143421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1044,"text":"wsp1420 - 1960 - Floods of August-October 1955, New England to North Carolina","interactions":[],"lastModifiedDate":"2023-03-07T22:32:05.254743","indexId":"wsp1420","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1420","title":"Floods of August-October 1955, New England to North Carolina","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1420","usgsCitation":"Bogart, D.B., 1960, Floods of August-October 1955, New England to North Carolina: U.S. Geological Survey Water Supply Paper 1420, Report: ix, 854 p.; 6 Plates: 32.00 x 40.00 inches or smaller, https://doi.org/10.3133/wsp1420.","productDescription":"Report: ix, 854 p.; 6 Plates: 32.00 x 40.00 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":413814,"rank":9,"type":{"id":36,"text":"NGMDB Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe40","contributors":{"authors":[{"text":"Bogart, Dean Butler","contributorId":85157,"corporation":false,"usgs":true,"family":"Bogart","given":"Dean","email":"","middleInitial":"Butler","affiliations":[],"preferred":false,"id":143083,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1623,"text":"wsp1567 - 1960 - Surface water supply of the United States, 1958, Part 13, Snake River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1567","title":"Surface water supply of the United States, 1958, Part 13, Snake River Basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1567","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1958, Part 13, Snake River Basin: U.S. Geological Survey Water Supply Paper 1567, 273 p. :tables., https://doi.org/10.3133/wsp1567.","productDescription":"273 p. :tables.","costCenters":[],"links":[{"id":137186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1567/report-thumb.jpg"},{"id":26688,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1567/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6960a3","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":143905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2711,"text":"wsp1479 - 1960 - Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1479","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1479","title":"Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1479","usgsCitation":"Smith, R.O., 1960, Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho: U.S. Geological Survey Water Supply Paper 1479, v, 68 p. :maps (2 fold. col. in pocket) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1479.","productDescription":"v, 68 p. :maps (2 fold. col. in pocket) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":139062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1479/report-thumb.jpg"},{"id":29090,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1479/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29091,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1479/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29092,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1479/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8efe","contributors":{"authors":[{"text":"Smith, Rex Onis","contributorId":93889,"corporation":false,"usgs":true,"family":"Smith","given":"Rex","email":"","middleInitial":"Onis","affiliations":[],"preferred":false,"id":145647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3565,"text":"cir429 - 1960 - Water-resources summary for southern California, 1959","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"429","title":"Water-resources summary for southern California, 1959","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir429","usgsCitation":"Peterson, W.C., 1960, Water-resources summary for southern California, 1959: U.S. Geological Survey Circular 429, iii, 10 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir429.","productDescription":"iii, 10 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":117709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0429/report-thumb.jpg"},{"id":30593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4db6","contributors":{"authors":[{"text":"Peterson, William C.","contributorId":54970,"corporation":false,"usgs":true,"family":"Peterson","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":178,"text":"wsp1450 - 1960 - Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1450","title":"Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1450","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1960, Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1450, xv, 603 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1450.","productDescription":"xv, 603 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1450/report-thumb.jpg"},{"id":24789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651d4f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3817,"text":"cir434 - 1960 - Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"434","title":"Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona","docAbstract":"Measurements of streamflow, ground-water levels, and meterological data obtained in a 4.1-mile reach of the flood plain of Cottonwood Wash, Mohave County, Ariz., define the use of water by riparian vegetation in that part of the stream valley. The computed evapotranspiration loss during the growing season of 1959 was 175 acre-feet, which represented about 33 percent of the water that entered the reach. The maximum rate of loss during the season was slightly more than 8 acre-feet per week, or about 60 percent of the inflow. \r\n\r\nThe project reach is divided into two parts: An upstream subreach of 2.6 miles and a downstream subreach of 1.5 miles. Seasonal losses in the upstream and downstream subreaches were 75 and 100 acre-feet respectively. Losses in the shorter downstream subreach were larger because of the greater plant population. \r\n\r\nDuring the summer of 1960 the vegetation in the lower subreach will be chemically defoliated as a part of the experiment to determine the savings in water losses that can be effected by modifying riparian vegetation. Tests on chemical defoliants indicate that a single spraying eliminates the leaves on cottonwood trees for 7 or 8 days and that no permanent damage results.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir434","usgsCitation":"Hendricks, E.L., Kam, W., and Bowie, J.E., 1960, Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona: U.S. Geological Survey Circular 434, iii, 11 p. :ill., map ;27 cm., https://doi.org/10.3133/cir434.","productDescription":"iii, 11 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":124664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0434/report-thumb.jpg"},{"id":30887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0434/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6493f4","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kam, William","contributorId":85159,"corporation":false,"usgs":true,"family":"Kam","given":"William","email":"","affiliations":[],"preferred":false,"id":147661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowie, James E.","contributorId":29393,"corporation":false,"usgs":true,"family":"Bowie","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147659,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4177,"text":"cir431 - 1960 - Wetland and water supply","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"431","title":"Wetland and water supply","docAbstract":"The Geological Survey has received numerous inquiries about the effects of proposed changes in the wetland environment. The nature of the inquiries suggests a general confusion in the public mind as to wetland values and an increasing concern by the public with the need for facts as a basis for sound decisions when public action is required. \r\n\r\nPerhaps the largest gap in our knowledge is in regard to the role played by the wetland in the natural water scheme. Specialists in such fields as agriculture and conservation have studied the wetland in relation to its special uses and values for farming and as a habitat for fish and wildlife. However, except as studied incidentally by these specialists, the role of the wetland with respect to water has been largely neglected. This facet of the wetland problem is of direct concern to the Geological Survey. \r\n\r\nWe commonly speak of water in terms of its place in the hydrologic environment---as, for example, surface water or ground water. These terms imply that water can be neatly pigeonholed. With respect to the wetland environment nothing can be further from the truth. In fact, one objective of this discussion is to demonstrate that for the wetland environment surface water, ground water, and soil water cannot be separated realistically, but are closely interrelated and must be studied together. It should be noted that this statement holds true for the hydrologic environment in general, and that the wetland environment is by no means unique in this respect. Our second and principal objective is to identify some of the problems that must be studied in order to clarify the role of the wetland in relation to water supply. \r\n\r\nWe have chosen to approach these objectives by briefly describing one area for which we have some information, and by using this example to point out some of the problems that need study. First, however, let us define what we, as geohydrologists, mean by wetland and briefly consider wetland classifications. \r\n\r\nFor our purpose wetlands are land areas that are covered with shallow water or subjected to intermittent flooding and subsequent slow drainage, and which generally are characterized by an accumulation of organic matter hereafter termed \u001Cswamp deposits.' These wetlands may be classified in a number of different ways depending on the purpose of the classifier. For example, the Fish and Wildlife Service classifies wetlands into 20 different types based on water quality (fresh or salty), drainage, and vegetation. At the risk of some oversimplification we might consider 4 types of wetland from the standpoint of hydrology: (1) fresh-water swamps in which the swamp deposits are underlain by glacial till or bedrock; (2)fresh-water swamps in which the swamp deposits are underlain by marine or lacustrine clay and silt; (3) fresh-water swamps in which the swamp deposits are underlain by glacial outwash or alluvium consisting mostly of sand or sand and gravel; and (4) salt .marshes and salt meadows. The three fresh-water types of wetland are of interest with respect to water supply, and of these, the type in which swamp deposits are underlain by glacial outwash is of particular interest in New England. \r\n\r\nIn the Ipswich River basin above the Geological Survey gaging station at South Middleton, Mass., is an area of 44 square miles which forms the headwaters section of the basin. The relief of the area is low. About half the area consists of hills mostly underlain by bedrock but mantled by a thin layer of glacial till. The other half consists Of lowlands---including swamps, low terraces and plains---underlain by glacial outwash, Swampland, used hereafter as a synonym for wetland, forms about a fourth of the area. Some of the swamps occupy depressions in the till blanket and are situated at somewhat higher levels than the lowlands. The largest swamps, however, border the Ipswich River and its tributaries. Here the swamp deposits, which consist of muck and peat mixed with s","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir431","usgsCitation":"Baker, J.A., 1960, Wetland and water supply: U.S. Geological Survey Circular 431, 3 p. ;27 cm., https://doi.org/10.3133/cir431.","productDescription":"3 p. ;27 cm.","costCenters":[],"links":[{"id":117878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0431/report-thumb.jpg"},{"id":31289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0431/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db545334","contributors":{"authors":[{"text":"Baker, John Augustus","contributorId":48159,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"Augustus","affiliations":[],"preferred":false,"id":148348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":180,"text":"wsp1520 - 1960 - Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1520","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1520","title":"Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1520","usgsCitation":"Love, S.K., 1960, Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1520, xvi, 641 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1520.","productDescription":"xvi, 641 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1520/report-thumb.jpg"},{"id":24791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1520/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651cd9","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2958,"text":"wsp1624 - 1960 - Surface water supply of the United States, 1959, Part 2-B, South Atlantic slope and eastern Gulf of Mexico Basins, Ogeechee River to Pearl River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1624","title":"Surface water supply of the United States, 1959, Part 2-B, South Atlantic slope and eastern Gulf of Mexico Basins, Ogeechee River to Pearl River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1624","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 2-B, South Atlantic slope and eastern Gulf of Mexico Basins, Ogeechee River to Pearl River: U.S. Geological Survey Water Supply Paper 1624, x, 488 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1624.","productDescription":"x, 488 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1624/report-thumb.jpg"},{"id":29667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1624/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943a2","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3938,"text":"cir436 - 1960 - Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho","interactions":[],"lastModifiedDate":"2013-07-24T14:28:49","indexId":"cir436","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"436","title":"Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho","docAbstract":"The Salmon Falls area contains about 80,000 acres of irrigable land, of which about 30,000 acres receives some water from the distribution system of Salmon River Canal Co., Ltd. This system utilizes virtually all the available surface water. A substantial amount of surface water, estimated to be about 70,000 acre-feet annually, is lost by leakage from the reservoir and the distribution system. Some of this water could be salvaged by lining sections of the canal where excessive losses occur. Ground water has not been extensively developed in the area, but some successful irrigation wells furnished supplemental irrigation water. Recharge to the area is from precipitation on the area, seepage from peripheral streams, seepage losses from the reservoir and canal system, irrigation seepage, and ground-water underflow. Ground water leaves the area by undertow to the north and northwest, and eventually reaches the Snake River. The total mount of underflow from the area was estimated by three different methods to be 17,000, 100,000, and 170,000 acre-feet per year. The preliminary estimate of 100,000 acre-feet was derived by the inventory of recharge and is probably more accurate than the other two methods. Calculations, based on estimates of transmissibility computed from specific capacities of wells, suggest that there may be some channels or conduits of higher than average transmissibility through which a large part of the undertow leaves the area, Possibly 25 percent of the ground-water outflow could be intercepted by wells. However, in part of the area the depth to water may be excessive for economic development. Chemical analyses of 25 samples of ground water indicate that most of the water sampled is suitable for irrigation. The samples found least suitable were of water occurring at shallow depth, south and east of Hollister.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir436","usgsCitation":"Fowler, K.H., 1960, Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho: U.S. Geological Survey Circular 436, Document: iii, 17 p.; 1 Map: 14.22 x 15.24 inches, https://doi.org/10.3133/cir436.","productDescription":"Document: iii, 17 p.; 1 Map: 14.22 x 15.24 inches","numberOfPages":"21","costCenters":[],"links":[{"id":124626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0436/report-thumb.jpg"},{"id":31023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0436/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271073,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0436/plate-1.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.04,41.99 ], [ -115.04,42.9 ], [ -114.0,42.9 ], [ -114.0,41.99 ], [ -115.04,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e11e","contributors":{"authors":[{"text":"Fowler, Kenneth H.","contributorId":23930,"corporation":false,"usgs":true,"family":"Fowler","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":147861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2154,"text":"wsp1524 - 1960 - Quality of surface water for irrigation, western United States, 1957","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1524","title":"Quality of surface water for irrigation, western United States, 1957","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1524","usgsCitation":"Love, S.K., 1960, Quality of surface water for irrigation, western United States, 1957: U.S. Geological Survey Water Supply Paper 1524, viii, 183 p., [1] folded leaf of plates :ill., map ;25 cm., https://doi.org/10.3133/wsp1524.","productDescription":"viii, 183 p., [1] folded leaf of plates :ill., map ;25 cm.","costCenters":[],"links":[{"id":137846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1524/report-thumb.jpg"},{"id":27764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1524/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654cf7","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2153,"text":"wsp1485 - 1960 - Quality of surface waters for irrigation, western United States, 1956","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1485","title":"Quality of surface waters for irrigation, western United States, 1956","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1485","usgsCitation":"Love, S.K., 1960, Quality of surface waters for irrigation, western United States, 1956: U.S. Geological Survey Water Supply Paper 1485, viii, 185 p. :ill, map ;25 cm., https://doi.org/10.3133/wsp1485.","productDescription":"viii, 185 p. :ill, map ;25 cm.","costCenters":[],"links":[{"id":137845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1485/report-thumb.jpg"},{"id":27763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651db1","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3139,"text":"wsp1558 - 1960 - Surface water supply of the United States, 1958, Part 5, Hudson Bay and upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp1558","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1558","title":"Surface water supply of the United States, 1958, Part 5, Hudson Bay and upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1558","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1958, Part 5, Hudson Bay and upper Mississippi River basins: U.S. Geological Survey Water Supply Paper 1558, xii, 638 p. :tables ;23 cm., https://doi.org/10.3133/wsp1558.","productDescription":"xii, 638 p. :tables ;23 cm.","costCenters":[],"links":[{"id":139429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1558/report-thumb.jpg"},{"id":30050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1558/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696074","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3752,"text":"cir433 - 1960 - Time, distance, and drawdown relationships in a pumped ground-water basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"433","title":"Time, distance, and drawdown relationships in a pumped ground-water basin","docAbstract":"Several reasonable values are assumed for coefficients of transmissibility and storage of lenticular alluvial deposits, These values when substituted in the Theis (1935) nonequilibrium formula as modified by Wenzel (1942) give curves from which time, distance, drawdown relationships are estimated.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir433","usgsCitation":"Kunkel, F., 1960, Time, distance, and drawdown relationships in a pumped ground-water basin: U.S. Geological Survey Circular 433, 8 p. :ill. ;27 cm. + graphs in back pocket., https://doi.org/10.3133/cir433.","productDescription":"8 p. :ill. ;27 cm. + graphs in back pocket.","costCenters":[],"links":[{"id":118313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0433/report-thumb.jpg"},{"id":30813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db49671f","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":147534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2057,"text":"wsp1495 - 1960 - Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1495","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1495","title":"Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California","docAbstract":"Napa and Sonoma Valleys are adjacent alluvium-filled valleys about 40 miles northeast of San Francisco. They occupy alined and structurally controlled depressions in the northern Coast Ranges physiographic province and drain south into San Pablo Bay. The valleys are surrounded and underlain by unconsolidated marine and continental sediments and volcanic rocks of Pliocene and Pleistocene age, which are water bearing in large part and together make up relatively extensive ground-water basins. Napa Valley, the eastern valley, is the larger and has a valley-floor area of about 85 square miles. Sonoma Valley has a valley-floor area of about 35 square miles; in addition, about 10 square miles is unreclaimed tidal marsh. \r\n\r\nThe rock units of Napa and Sonoma Valleys are divided into four classes on the basis of their distribution and relative capacity to yield water: (a) Consolidated virtually non-water-bearing chiefly sedimentary (some metamorphic) rocks that range in age from Jurassic ( ?) to Pliocene; (b) marine shale and sand of the Petaluma formation (Pliocene) and the Merced formation (Pliocene and Pleistocene) that do not crop out within Napa or Sonoma Valleys but perhaps are penetrated by some deep wells drilled in Sonoma Valley; (c) Sonoma volcanics of Pliocene age, parts of which are non-water-bearing and parts of which locally yield large quantities of water; and (d) unconsolidated alluvial deposits mainly of Quaternary age. The deposits of classes (c) and (d) contain the most important aquifers in the area. \r\n\r\nMost of the water used in these valleys is pumped from wells in the younger and older alluvium in the Huichica and Glen Ellen formations. and in the Sonoma volcanics. The principal aquifers are the younger and older alluvium. but appreciable quantities of water are pumped locally from the Sonoma volcanics. The Huichica and Glen Ellen formations yield water in small quantities and at most places supply water only for limited domestic uses. \r\n\r\nThe younger alluvium COIM3ists of interbedded deposits of unconsolidated gravel. sand, silt. and. locally, peat. These deposits underlie the flood plains and channels of the Napa River. Sonoma Creek, and their tributaries, low alluvial fans or plains graded to these streams. and the tidal marshlands. The older alluvium of Napa and Sonoma Valleys is composed of lenticular deposits of unconsolidated and poorly sorted clay, silt. sand. and gravel. Where exposed, claypan or hardpan soil is characteristically developed at the surface. \r\n\r\nThe Huichica formation is composed of deformed continental beds consisting mostly of yellow silt with some interbedded lenses of silt and gravel, and silt and boulders. At the base are beds of redeposited volcanic material, silt, clay, and lenses of coarse gravel and boulders. The Glen Ellen fcrmation consists of alluvial clay, silt, sand, and gravel in clearly stratified but generally lenticular beds. The Sonoma volcanics constitute a thick and highly variate series of continental volcanic rocks, including andesite, basalt, and minor rhyolite flows and interbedded coarse- to fine-grained pyroclastic tuff and breccia, redeposited tuff and pumice, and diatomaceous mud, silt, and sand. A prominent body of rhyolite flows and tuff with some obsidian and perlitic glass, called the St. Helena rhyolite member, occurs in the upper part. \r\n\r\nEstimated ground-water pumpage for all uses in the year 1949-50 was about 5,600 acre-feet in Napa Valley and about 2,400 acre-feet in Sonoma Valley. Of this quantity the amounts pumped for irrigation were about 2,900 and 1,900 acre-feet, respectively. \r\n\r\nWater levels in wells in the central parts of the valleys range from a few feet above the land surface to about 50 feet below, with an average of about 25 feet. The quality of the water in most wells is satisfactory for domestic use and irrigation. Locally at the southern end of the valley some contamination of the native waters is caused by the movement of salty wate","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1495","usgsCitation":"Kunkel, F., and Upson, J.E., 1960, Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California: U.S. Geological Survey Water Supply Paper 1495, v, 252 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1495.","productDescription":"v, 252 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1495/report-thumb.jpg"},{"id":27593,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27594,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27595,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27596,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27597,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1495/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db68604a","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":144610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Upson, Joseph Edwin","contributorId":21528,"corporation":false,"usgs":true,"family":"Upson","given":"Joseph","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":144609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}